摘要
Many types of oncoids,which have great significance for sedimentary environment research, are well developed in Paleogene Guanzhuang Formation in Pingyi Basin. Based on previous studies,the morphometry,structure,fossil,texture and the characteristics of geochemistry of the oncolites in host area were analyzed by means of field inspection,microscope observation and geochemical test. Based this study,the oncoids were divided into Type A and Type B,and the most fundamental difference between them lies in sedimentary environments where they originated.According to above study,the oncolites developed in a close,dry and hot lake,which was on the stage of transgression.